Climate sensitivity and drought seasonality determine post-drought growth recovery of Quercus petraea and Quercus robur in Europe
Recent studies have identified strong relationships between delayed recovery of tree growth after drought and tree mortality caused by subsequent droughts. These observations raise concerns about forest ecosystem services and post-drought growth recovery given the projected increase in drought frequ...
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creator | Bose, Arun K. Scherrer, Daniel Camarero, J. Julio Ziche, Daniel Babst, Flurin Bigler, Christof Bolte, Andreas Dorado-Liñán, Isabel Etzold, Sophia Fonti, Patrick Forrester, David I. Gavinet, Jordane Gazol, Antonio de Andrés, Ester González Karger, Dirk Nikolaus Lebourgeois, Francois Lévesque, Mathieu Martínez-Sancho, Elisabet Menzel, Annette Neuwirth, Burkhard Nicolas, Manuel Sanders, Tanja G.M. Scharnweber, Tobias Schröder, Jens Zweifel, Roman Gessler, Arthur Rigling, Andreas |
description | Recent studies have identified strong relationships between delayed recovery of tree growth after drought and tree mortality caused by subsequent droughts. These observations raise concerns about forest ecosystem services and post-drought growth recovery given the projected increase in drought frequency and extremes. For quantifying the impact of extreme droughts on tree radial growth, we used a network of tree-ring width data of 1689 trees from 100 sites representing most of the distribution of two drought tolerant, deciduous oak species (Quercus petraea and Quercus robur). We first examined which climatic factors and seasons control growth of the two species and if there is any latitudinal, longitudinal or elevational trend. We then quantified the relative departure from pre-drought growth during droughts, and how fast trees were able to recover the pre-drought growth level. Our results showed that growth was more related to precipitation and climatic water balance (precipitation minus potential evapotranspiration) than to temperature. However, we did not detect any clear latitudinal, longitudinal or elevational trends except a decreasing influence of summer water balance on growth of Q. petraea with latitude. Neither species was able to maintain the pre-drought growth level during droughts. However, both species showed rapid recovery or even growth compensation after summer droughts but displayed slow recovery in response to spring droughts where none of the two species was able to fully recover the pre-drought growth-level over the three post-drought years. Collectively, our results indicate that oaks which are considered resilient to extreme droughts have also shown vulnerability when droughts occurred in spring especially at sites where long-term growth is not significantly correlated with climatic factors. This improved understanding of the role of drought seasonality and climate sensitivity of sites is key to better predict trajectories of post-drought growth recovery in response to the drier climate projected for Europe.
[Display omitted]
•Quercus petraea and Q. robur responses to extreme droughts were examined.•Growth was more related to precipitation compared to temperature.•Droughts occurred in previous winter and current spring had greater impact.•Neither species able to recover the pre-drought growth levels to spring droughts•Long-term growth-climate relationship measured the responses to extreme droughts. |
doi_str_mv | 10.1016/j.scitotenv.2021.147222 |
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[Display omitted]
•Quercus petraea and Q. robur responses to extreme droughts were examined.•Growth was more related to precipitation compared to temperature.•Droughts occurred in previous winter and current spring had greater impact.•Neither species able to recover the pre-drought growth levels to spring droughts•Long-term growth-climate relationship measured the responses to extreme droughts.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2021.147222</identifier><identifier>PMID: 34088042</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Acclimation ; Biodiversity and Ecology ; Climate change ; Drought ; Environmental Sciences ; Global Changes ; Legacy effects ; Tree rings ; Warming</subject><ispartof>The Science of the total environment, 2021-08, Vol.784, p.147222-147222, Article 147222</ispartof><rights>2021 The Authors</rights><rights>Attribution</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c431t-21c31f6fc62af777ce8d081cdcf1051a0e9f14870e48117239ee16b49aa4d0543</citedby><cites>FETCH-LOGICAL-c431t-21c31f6fc62af777ce8d081cdcf1051a0e9f14870e48117239ee16b49aa4d0543</cites><orcidid>0000-0002-0885-1227 ; 0000-0002-2040-6150</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.scitotenv.2021.147222$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>230,314,780,784,885,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttps://agroparistech.hal.science/hal-03880251$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Bose, Arun K.</creatorcontrib><creatorcontrib>Scherrer, Daniel</creatorcontrib><creatorcontrib>Camarero, J. Julio</creatorcontrib><creatorcontrib>Ziche, Daniel</creatorcontrib><creatorcontrib>Babst, Flurin</creatorcontrib><creatorcontrib>Bigler, Christof</creatorcontrib><creatorcontrib>Bolte, Andreas</creatorcontrib><creatorcontrib>Dorado-Liñán, Isabel</creatorcontrib><creatorcontrib>Etzold, Sophia</creatorcontrib><creatorcontrib>Fonti, Patrick</creatorcontrib><creatorcontrib>Forrester, David I.</creatorcontrib><creatorcontrib>Gavinet, Jordane</creatorcontrib><creatorcontrib>Gazol, Antonio</creatorcontrib><creatorcontrib>de Andrés, Ester González</creatorcontrib><creatorcontrib>Karger, Dirk Nikolaus</creatorcontrib><creatorcontrib>Lebourgeois, Francois</creatorcontrib><creatorcontrib>Lévesque, Mathieu</creatorcontrib><creatorcontrib>Martínez-Sancho, Elisabet</creatorcontrib><creatorcontrib>Menzel, Annette</creatorcontrib><creatorcontrib>Neuwirth, Burkhard</creatorcontrib><creatorcontrib>Nicolas, Manuel</creatorcontrib><creatorcontrib>Sanders, Tanja G.M.</creatorcontrib><creatorcontrib>Scharnweber, Tobias</creatorcontrib><creatorcontrib>Schröder, Jens</creatorcontrib><creatorcontrib>Zweifel, Roman</creatorcontrib><creatorcontrib>Gessler, Arthur</creatorcontrib><creatorcontrib>Rigling, Andreas</creatorcontrib><title>Climate sensitivity and drought seasonality determine post-drought growth recovery of Quercus petraea and Quercus robur in Europe</title><title>The Science of the total environment</title><description>Recent studies have identified strong relationships between delayed recovery of tree growth after drought and tree mortality caused by subsequent droughts. These observations raise concerns about forest ecosystem services and post-drought growth recovery given the projected increase in drought frequency and extremes. For quantifying the impact of extreme droughts on tree radial growth, we used a network of tree-ring width data of 1689 trees from 100 sites representing most of the distribution of two drought tolerant, deciduous oak species (Quercus petraea and Quercus robur). We first examined which climatic factors and seasons control growth of the two species and if there is any latitudinal, longitudinal or elevational trend. We then quantified the relative departure from pre-drought growth during droughts, and how fast trees were able to recover the pre-drought growth level. Our results showed that growth was more related to precipitation and climatic water balance (precipitation minus potential evapotranspiration) than to temperature. However, we did not detect any clear latitudinal, longitudinal or elevational trends except a decreasing influence of summer water balance on growth of Q. petraea with latitude. Neither species was able to maintain the pre-drought growth level during droughts. However, both species showed rapid recovery or even growth compensation after summer droughts but displayed slow recovery in response to spring droughts where none of the two species was able to fully recover the pre-drought growth-level over the three post-drought years. Collectively, our results indicate that oaks which are considered resilient to extreme droughts have also shown vulnerability when droughts occurred in spring especially at sites where long-term growth is not significantly correlated with climatic factors. This improved understanding of the role of drought seasonality and climate sensitivity of sites is key to better predict trajectories of post-drought growth recovery in response to the drier climate projected for Europe.
[Display omitted]
•Quercus petraea and Q. robur responses to extreme droughts were examined.•Growth was more related to precipitation compared to temperature.•Droughts occurred in previous winter and current spring had greater impact.•Neither species able to recover the pre-drought growth levels to spring droughts•Long-term growth-climate relationship measured the responses to extreme droughts.</description><subject>Acclimation</subject><subject>Biodiversity and Ecology</subject><subject>Climate change</subject><subject>Drought</subject><subject>Environmental Sciences</subject><subject>Global Changes</subject><subject>Legacy effects</subject><subject>Tree rings</subject><subject>Warming</subject><issn>0048-9697</issn><issn>1879-1026</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNqFkUFr3DAQhUVoaLZpf0N0bA_eamStJR-XJWkCC6WQnoUij7NavJYryS57zD-vXDe5di4Dj28ezHuE3ABbA4Pq63EdrUs-YT-tOeOwBiE55xdkBUrWBTBevSMrxoQq6qqWV-RDjEeWRyp4T65KwZRigq_Iy65zJ5OQRuyjS25y6UxN39Am-PH5kLJuou9NN-sNJgwn1yMdfEzFK_Ic_O90oAGtnzCcqW_pjxGDHSMdMAWD5q_jqxb80xio6-ntGPyAH8lla7qIn_7ta_Lz7vZxd1_sv3972G33hRUlpIKDLaGtWltx00opLaqGKbCNbYFtwDCsWxBKMhQKQPKyRoTqSdTGiIZtRHlNviy-B9PpIeSvw1l74_T9dq9njZU5E76BCTL7eWGH4H-NGJM-uWix60yPfoyab0pZibLkVUblgtrgYwzYvnkD03NX-qjfutJzV3rpKl9ul0vMX08Ow8xhb7FxOcqkG-_-6_EHXGyiEw</recordid><startdate>20210825</startdate><enddate>20210825</enddate><creator>Bose, Arun K.</creator><creator>Scherrer, Daniel</creator><creator>Camarero, J. 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Julio ; Ziche, Daniel ; Babst, Flurin ; Bigler, Christof ; Bolte, Andreas ; Dorado-Liñán, Isabel ; Etzold, Sophia ; Fonti, Patrick ; Forrester, David I. ; Gavinet, Jordane ; Gazol, Antonio ; de Andrés, Ester González ; Karger, Dirk Nikolaus ; Lebourgeois, Francois ; Lévesque, Mathieu ; Martínez-Sancho, Elisabet ; Menzel, Annette ; Neuwirth, Burkhard ; Nicolas, Manuel ; Sanders, Tanja G.M. ; Scharnweber, Tobias ; Schröder, Jens ; Zweifel, Roman ; Gessler, Arthur ; Rigling, Andreas</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c431t-21c31f6fc62af777ce8d081cdcf1051a0e9f14870e48117239ee16b49aa4d0543</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Acclimation</topic><topic>Biodiversity and Ecology</topic><topic>Climate change</topic><topic>Drought</topic><topic>Environmental Sciences</topic><topic>Global Changes</topic><topic>Legacy effects</topic><topic>Tree rings</topic><topic>Warming</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bose, Arun K.</creatorcontrib><creatorcontrib>Scherrer, Daniel</creatorcontrib><creatorcontrib>Camarero, J. 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Julio</au><au>Ziche, Daniel</au><au>Babst, Flurin</au><au>Bigler, Christof</au><au>Bolte, Andreas</au><au>Dorado-Liñán, Isabel</au><au>Etzold, Sophia</au><au>Fonti, Patrick</au><au>Forrester, David I.</au><au>Gavinet, Jordane</au><au>Gazol, Antonio</au><au>de Andrés, Ester González</au><au>Karger, Dirk Nikolaus</au><au>Lebourgeois, Francois</au><au>Lévesque, Mathieu</au><au>Martínez-Sancho, Elisabet</au><au>Menzel, Annette</au><au>Neuwirth, Burkhard</au><au>Nicolas, Manuel</au><au>Sanders, Tanja G.M.</au><au>Scharnweber, Tobias</au><au>Schröder, Jens</au><au>Zweifel, Roman</au><au>Gessler, Arthur</au><au>Rigling, Andreas</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Climate sensitivity and drought seasonality determine post-drought growth recovery of Quercus petraea and Quercus robur in Europe</atitle><jtitle>The Science of the total environment</jtitle><date>2021-08-25</date><risdate>2021</risdate><volume>784</volume><spage>147222</spage><epage>147222</epage><pages>147222-147222</pages><artnum>147222</artnum><issn>0048-9697</issn><eissn>1879-1026</eissn><abstract>Recent studies have identified strong relationships between delayed recovery of tree growth after drought and tree mortality caused by subsequent droughts. These observations raise concerns about forest ecosystem services and post-drought growth recovery given the projected increase in drought frequency and extremes. For quantifying the impact of extreme droughts on tree radial growth, we used a network of tree-ring width data of 1689 trees from 100 sites representing most of the distribution of two drought tolerant, deciduous oak species (Quercus petraea and Quercus robur). We first examined which climatic factors and seasons control growth of the two species and if there is any latitudinal, longitudinal or elevational trend. We then quantified the relative departure from pre-drought growth during droughts, and how fast trees were able to recover the pre-drought growth level. Our results showed that growth was more related to precipitation and climatic water balance (precipitation minus potential evapotranspiration) than to temperature. However, we did not detect any clear latitudinal, longitudinal or elevational trends except a decreasing influence of summer water balance on growth of Q. petraea with latitude. Neither species was able to maintain the pre-drought growth level during droughts. However, both species showed rapid recovery or even growth compensation after summer droughts but displayed slow recovery in response to spring droughts where none of the two species was able to fully recover the pre-drought growth-level over the three post-drought years. Collectively, our results indicate that oaks which are considered resilient to extreme droughts have also shown vulnerability when droughts occurred in spring especially at sites where long-term growth is not significantly correlated with climatic factors. This improved understanding of the role of drought seasonality and climate sensitivity of sites is key to better predict trajectories of post-drought growth recovery in response to the drier climate projected for Europe.
[Display omitted]
•Quercus petraea and Q. robur responses to extreme droughts were examined.•Growth was more related to precipitation compared to temperature.•Droughts occurred in previous winter and current spring had greater impact.•Neither species able to recover the pre-drought growth levels to spring droughts•Long-term growth-climate relationship measured the responses to extreme droughts.</abstract><pub>Elsevier B.V</pub><pmid>34088042</pmid><doi>10.1016/j.scitotenv.2021.147222</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-0885-1227</orcidid><orcidid>https://orcid.org/0000-0002-2040-6150</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Acclimation Biodiversity and Ecology Climate change Drought Environmental Sciences Global Changes Legacy effects Tree rings Warming |
title | Climate sensitivity and drought seasonality determine post-drought growth recovery of Quercus petraea and Quercus robur in Europe |
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